Fig. 17From: Crustal structure of the eastern Piedmont and Atlantic coastal plain in North Carolina and Virginia, eastern North American marginP-wave velocity structure beneath south China (a) and the margin of the South China Sea (b). We merge these two crustal models a, b to make the composite section in Fig. 18a. c the P-wave velocity structure crossing Kenya Rift. Locations of these seismic profiles are indicated in Fig. 16Back to article page